Knowledge Management System Of Institute of Oceanology, Chinese Academy of Sciences
The influence of oceanic anoxic events on convergent margin magmas | |
Wang, Kun1,2,3; Zhang, Li-Peng1,3; Deng, Jiang-Hong1,3; Sui, Qing-Lin1,2,3; Xie, Guo-Zhi1,2,3; Sun, Wei-Dong1,2,3 | |
2021-12-15 | |
发表期刊 | LITHOS |
ISSN | 0024-4937 |
卷号 | 406-407页码:6 |
通讯作者 | Zhang, Li-Peng([email protected]) |
摘要 | In general, the arc magmas are oxidized, forming magnetite-series granitoids. However, there are also ilmeniteseries granitoids at convergent margins. The mechanism that controls the formation of different types of granitoids remains obscure. Here we show that the temporal distributions of ilmenite-series granitoids in Japan have a good correlation with oceanic anoxic events (OAEs). The subduction of OAE sediments with high contents of organic matters releases reducing fluids/melts into the mantle wedge, leading to the formation of ilmenite-series granitoids. This is supported by sulfur isotope compositions and high concentrations of organic gas of the ilmenite-series granitoids in Japan. The temporal correlation between OAEs and Il-series granitoids suggests that the OAE sediments was predominantly distributed within short distances (<2000 km) along the coast. Considerable amount of organic matters are recycled back to the surface during plate subduction, and thus have major influences on carbon recycling, and climate changes, as well as oxygen fugacity of convergent margin magmas and associated mineralizations. |
关键词 | Magnetite-series Ilmenite-series Oceanic anoxic events Granitoid Japan |
DOI | 10.1016/j.lithos.2021.106529 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | Strategic Priority Research Program of the Chinese Academy of Sciences[XDA22050103]; National Natural Science Foundation of China[41803032]; Taishan Scholar Program of Shandong[ts201712075] |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
WOS类目 | Geochemistry & Geophysics ; Mineralogy |
WOS记录号 | WOS:000722656600003 |
出版者 | ELSEVIER |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/177306 |
专题 | 深海极端环境与生命过程研究中心 |
通讯作者 | Zhang, Li-Peng |
作者单位 | 1.Chinese Acad Sci, Ctr Ocean Mega Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Pilot Natl Lab Marine Sci & Technol Qingdao, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China |
第一作者单位 | 中国科学院海洋研究所 |
通讯作者单位 | 中国科学院海洋研究所 |
推荐引用方式 GB/T 7714 | Wang, Kun,Zhang, Li-Peng,Deng, Jiang-Hong,et al. The influence of oceanic anoxic events on convergent margin magmas[J]. LITHOS,2021,406-407:6. |
APA | Wang, Kun,Zhang, Li-Peng,Deng, Jiang-Hong,Sui, Qing-Lin,Xie, Guo-Zhi,&Sun, Wei-Dong.(2021).The influence of oceanic anoxic events on convergent margin magmas.LITHOS,406-407,6. |
MLA | Wang, Kun,et al."The influence of oceanic anoxic events on convergent margin magmas".LITHOS 406-407(2021):6. |
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文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
1-s2.0-S002449372100(6370KB) | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 |
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